Hypoxia-related processes in the Baltic Sea.
By D. Conley, S. Björck, E. Bonsdorff, J. Carstensen, G. Destouni, B. Gustafsson, S. Hietanen, M. Kortekaas, H. Kuosa, H. Meier and 12 more. Environmental Science and Technology, 2009
596 citations recorded by the source corpus.
View Paper: https://www.semanticscholar.org/paper/5fde44afbd8035f1dc59367fb2a8e9e9eafd7585
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Citations in the corpus
- Hypoxic areas, density-dependence and food limitation drive the body condition of a heavily exploited marine fish predator (2016, methodology): “Hypoxic areas were also used in our study as an indicator of benthic productivity [48,49] and thus of cod benthic feeding opportunities.”
- Deoxygenation of the Baltic Sea during the last century (2014, background): “In the Baltic Sea, the present spread of hypoxia is the combined result of climate changes influencing deepwater oxygenation (6) and increased eutrophication (7, 8), resulting in a hypoxic area ranging between 12,000 and 70,000 km(2) with an average of 49,000 km(2) over the time period 1961–2000 (7)”
- Comparing reconstructed past variations and future projections of the Baltic Sea ecosystem—first results from multi-model ensemble simulations (2012, background): “As a consequence, the Baltic Sea today suffers from severe environmental problems due to eutrophication, e.g., extensive cyanobacteria blooms and an expansion of dead bottoms (e.g., Elmgren 2001, Conley et al 2009, Savchuk 2010).”
- In search of the dead zone: Use of otoliths for tracking fish exposure to hypoxia (2015, unknown): “The Baltic Sea, although historically subject to periodic hypoxia and anoxia episodes typically in deeper areas (Zillén et al., 2008), has increased incidence of seasonal hypoxia since the 1960s (Conley et al., 2009; Savchuk, 2010).”
- Occurrence of benthic microbial nitrogen fixation coupled to sulfate reduction in the seasonally hypoxic Eckernförde Bay, Baltic Sea (2012, background): “…Sea are highly variable and typically impacted by fluctuating hypoxia and macrofaunal presence (Karlson et al., 2005; Hietanen and Lukkari, 2007; Conley et al., 2009), and so a possibly inaccurate view of Eckernförde Bay benthic N cycling could be formed if comparing N2 fixation rates from…”
- Mini-review: A priori considerations for bacteria–algae interactions in algal biofuel systems receiving municipal wastewaters (2014, background): “phorous [104,106], stimulating sulphate reduction, inhibiting nitrification, and thus prolonging nitrogen retention in the system [82,104], and stimulating methanogenesis [84].”
- Diatom bloom‐derived bottom water hypoxia off the Changjiang estuary, with and without typhoon influence (2017, background): “Examples include the Chesapeake Bay (Hagy et al. 2004), Baltic Sea (Conley et al. 2009; Carstensen et al. 2014), Gulf of Mexico (Dagg et al. 2007; Rabalais et al. 2014), Pearl River (Cai et al. 2004; Dai et al. 2006), and Changjiang estuary (Li et al. 2002).”